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<article language="en">
	<journal>
		<journal_title>Hydrology and Earth System Sciences</journal_title>
		<journal_url>www.hydrol-earth-syst-sci.net</journal_url>
		<issn>1027-5606</issn>
		<eissn>1607-7938</eissn>
		<volume_number>13</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/hess-13-157-2009</doi>
	<article_url>http://www.hydrol-earth-syst-sci.net/13/157/2009/</article_url>
	<abstract_html>http://www.hydrol-earth-syst-sci.net/13/157/2009/hess-13-157-2009.html</abstract_html>
	<fulltext_pdf>http://www.hydrol-earth-syst-sci.net/13/157/2009/hess-13-157-2009.pdf</fulltext_pdf>
	<start_page>157</start_page>
	<end_page>161</end_page>
	<publication_date>2009-02-18</publication_date>
	<article_title content_type="html">&lt;i&gt;HESS Opinions&lt;/i&gt; &quot;The art of hydrology&quot;*</article_title>
	<authors>
		<author numeration="1" affiliations="1,2,3">
			<name>H. H. G. Savenije</name>
			<email>h.h.g.savenije@tudelft.nl</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Water Management, Delft University of Technology, Delft, The Netherlands</affiliation>
		<affiliation numeration="2" content_type="html">Unesco-IHE, Institute for Water Education, Delft, The Netherlands</affiliation>
		<affiliation numeration="3" content_type="html">Invited contribution by H. H. G. Savenije, EGU Henry Darcy Medal award 2008.</affiliation>
	</affiliations>
	<abstract content_type="html">Hydrological modelling is the same as developing and encoding a hydrological
theory. A hydrological model is not a tool but a hypothesis. The whole
discussion about the inadequacy of hydrological models we have witnessed of
late, is related to the wrong concept of what a model is. Good models don&apos;t
exist. Instead of looking for the &quot;best&quot; model, we should aim at developing
better models. The process of modelling should be top-down, learning from the
data while at the same time connection should be established with underlying
physical theory (bottom-up). As a result of heterogeneity occurring at all
scales in hydrology, there always remains a need for calibration of models.
This implies that we need tailor-made and site-specific models. Only flexible
models are fit for this modelling process, as opposed to most of the
established software or &quot;one-size-fits-all&quot; models. The process of
modelling requires imagination, inspiration, creativity, ingenuity,
experience and skill. These are qualities that belong to the field of art.
Hydrology is an art as much as it is science and engineering.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Beven, K. J.: Prophesy, reality and uncertainty in distributed hydrological modelling, Adv. Water Resour., 16, 41–51, 1993 </reference>
		<reference numeration="2" content_type="text"> Beven, K.: Towards integrated environmental models of everywhere: uncertainty, data and modelling as a learning process, Hydrol. Earth Syst. Sci., 11, 460–467, 2007. </reference>
		<reference numeration="3" content_type="text"> Fenicia, F., Savenije, H. H. G., and Avdeeva, Y.: Anomaly in the rainfall-runoff behaviour of the Meuse catchment. Climate, land use, or land use management?, Hydrol. Earth Syst. Sci. Discuss., 5, 1787–1819, 2008. </reference>
		<reference numeration="4" content_type="text"> Fenicia, F., Savenije, H H G., Matgen, P., and Pfister, L.: Understanding catchment behavior through stepwise model concept improvement, Water Resour. Res., 44, W01402, 1–13, doi:10.1029/2006WR005563, 2008b. </reference>
		<reference numeration="5" content_type="text"> Gumbricht, T., McCarthy, J., and McCarthy, T S.: Channels, wetlands and islands in the Okavango Delta, Botswana, and their relation to hydrological and sedimentological processes, Earth Surf. Proc. Land., 29(1), 15–29, 2004. </reference>
		<reference numeration="6" content_type="text"> Gumbricht, T., McCarthy, T S., and Bauer, P.: The micro-topography of the wetlands of the Okavango Delta, Botswana, Earth Surf. Proc. Land., 30(1), 27–39, 2005. </reference>
		<reference numeration="7" content_type="text"> Kinzelbach, W.: Hydrological Science and Engineering: the Yin and Yang of Water Resources Management, Geophysical Research Abstracts, Vol 10, EGU2008-A-10943, 2008. </reference>
		<reference numeration="8" content_type="text"> Savenije, H H G.: Equifinality, a blessing in disguise?, Hydrol. Process., 15, 2835–2838, 2001. </reference>
		<reference numeration="9" content_type="text"> Sivapalan, M., Blöschl, G., Zhang, L., and Vertessy, R.: Downward approach to hydrological prediction, Hydrol. Process., 17(11), 2101–2111, 2003. </reference>
		<reference numeration="10" content_type="text"> Wolski, P., Savenije, H H G., Murray-Hudson, M., and Gumbricht, T.: Modelling of the flooding in the Okavango Delta, Botswana, using a hybrid reservoir-GIS model, J. Hydrol., 331, 58–72, 2006. </reference>
	</references>
</article>

